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Sediment budget as affected by construction of a sequence of dams in the lower Red River, Viet Nam

机译:越南下游红河下游一系列水坝的建设影响了泥沙预算

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Dam construction is one of the main factors resulting in riverine sediment changes, which in turn cause river degradation or aggradation downstream. The main objective of this work is to examine the sediment budget affected by a sequence of dams constructed upstream in the lower reach of the Red River. The study is based on the longer-term annual data (1960-2010) with a complementary daily water and sediment data set (2008-2010). The results showed that the stretch of the river changed from sediment surplus (suggesting possible deposition processes) into sediment deficit (possible erosion processes) after the first dam (Thac Ba Dam) was constructed in 1972 and changed back to deposition after the second dam (Hoa Binh Dam) was constructed in 1985. The annual sediment deposition varied between 1.9 Mt/y and 46.7 Mt/y with an annual mean value of 22.9 Mt/y (1985-2010). The sediment deposition at the lower reach of the Red River would accelerate river aggradation which would change river channel capacity in the downstream of the Red River. The depositional processes could be sustained or changed back to erosional processes after more dams (the amount of sediment deposit was much less after the latest two dams Tuyen Quang Dam in 2009 and Sonia Dam in 2010) are constructed, depending on the water and sediment dynamics. This study revealed that the erosional and depositional processes could be shifted for the same stretch of river as affected by a sequence of dams and provides useful insights in river management in order to reduce flood frequency along the lower reach of the Red River. (C) 2015 Elsevier B.V. All rights reserved.
机译:大坝的建设是导致河流沉积物变化的主要因素之一,而河流沉积物的变化反过来又导致河流退化或下游的凝结。这项工作的主要目的是研究红河下游上游修建的一系列水坝对沉积物预算的影响。该研究基于长期的年度数据(1960-2010)和补充的每日水和泥沙数据集(2008-2010)。结果表明,在1972年建造了第一座水坝(Thac Ba Dam)之后,河流的延伸范围从沉积物过剩(暗示可能的沉积过程)变为沉积物不足(可能的侵蚀过程),并在第二座水坝(华平大坝(Hoa Binh Dam)建于1985年。年沉积物沉积量介于1.9 Mt / y和46.7 Mt / y之间,年平均值为22.9 Mt / y(1985-2010年)。红河下游的沉积物沉积会加速河水的沉积,从而改变红河下游的河道容量。取决于水和沉积物的动力学,在建造更多的水坝后(2009年最新的两个水坝Tuyen Quang大坝和2010年的Sonia大坝建成后,沉积过程可以维持或转变为侵蚀过程)。 。这项研究表明,在受一系列水坝影响的同一条河流中,侵蚀和沉积过程可能会发生变化,并为河流管理提供有用的见解,以减少红河下游的洪水频率。 (C)2015 Elsevier B.V.保留所有权利。

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